Isostasy is the flotational balance achieved between rocks of the crust lithosphere and deeper mantle. This balance is maintained as lighter rocks of the crust "float" on the denser rocks of the mantle below.
The force responsible for the Earth's crust and lithosphere floating on the mantle is isostasy. Isostasy is a balancing act between the buoyant force of the lithosphere on the denser, more fluid asthenosphere below it. This balance helps maintain the equilibrium of the Earth's crust.
lithosphere
The part of the Earth between the crust and the mantle is called the lithosphere. It includes the Earth's crust and the uppermost portion of the mantle, which together form a rigid layer. Below the lithosphere lies the asthenosphere, a semi-fluid layer of the mantle that allows for tectonic plate movement.
The region below the Earth's crust is called the mantle. It is composed of solid rock that is more rigid than the crust but less dense than the core. The mantle plays a key role in the movements of tectonic plates and the heat flow of the Earth.
Isostasy is the flotational balance achieved between rocks of the crust lithosphere and deeper mantle. This balance is maintained as lighter rocks of the crust "float" on the denser rocks of the mantle below.
The crust is above the mantle and the mantle is below the crust
Isostatic equilibrium is the balance between Earth's crust and the layer of mantle it floats on. The denser the crust is, the more it sinks into the mantle. Equilibrium is achieved when the crust floats at a certain level in the mantle.
The Earth's mantle is below the crust. The layers of the Earth form concentric spheres. Below the mantle is the core.
Mantle Is The Below Layer Of The Crust In Earth.
The force responsible for the Earth's crust and lithosphere floating on the mantle is isostasy. Isostasy is a balancing act between the buoyant force of the lithosphere on the denser, more fluid asthenosphere below it. This balance helps maintain the equilibrium of the Earth's crust.
The interior of the Earth, similar to the other terrestrial planets, is chemically divided into layers. The mantle is a highly viscous layer between the crust and the outer core. As such, the core (split into the solid inner and liquid outer layers) is below the mantle.
the mantle
lithosphere
The part of the Earth between the crust and the mantle is called the lithosphere. It includes the Earth's crust and the uppermost portion of the mantle, which together form a rigid layer. Below the lithosphere lies the asthenosphere, a semi-fluid layer of the mantle that allows for tectonic plate movement.
The zone between the core and crust of the Earth is the mantle. It is a layer of solid rock that extends about 1,800 miles (2,900 kilometers) below the Earth's surface. The mantle is made up of silicate minerals and is responsible for convection currents that drive plate tectonics.
15 kilo meters is the distance between the crust and the mantle